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Hydrogeochemical controls on the mobility of arsenic, fluoride and other geogenic co-contaminants in the shallow aquifers of northeastern La Pampa Province in Argentina

Aullón Alcaine, Anna (författare)
KTH,Hållbar utveckling, miljövetenskap och teknik
Schulz, Carlos (författare)
Univ Nacl La Pampa UNLPam, Fac Ciencias Exactas & Nat, Av Uruguay 151,L6300, Santa Rosa, La Pampa, Argentina.
Bundschuh, Jochen (författare)
Univ Southern Queensland, UNESCO Chair Groundwater Arsen Agenda Sustainable, West St, Toowoomba, Qld 4350, Australia.;Univ Southern Queensland, Fac Hlth Engn & Sci, West St, Toowoomba, Qld 4350, Australia.
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Jacks, Gunnar (författare)
KTH,Hållbar utveckling, miljövetenskap och teknik
Thunvik, Roger (författare)
KTH,Hållbar utveckling, miljövetenskap och teknik
Gustafsson, Jon Petter, 1964- (författare)
KTH,Vatten- och miljöteknik
Mörth, Carl-Magnus (författare)
Stockholms universitet,Institutionen för geologi och geokemi,Stockholm Univ, Dept Geol & Geochem, Stockholm, Sweden.
Sracek, Ondra (författare)
Palacky Univ, Fac Sci, Dept Geol, 17 Listopadu 12, Olomouc 777146, Czech Republic.
Ahmad, Arslan (författare)
KTH,Hållbar utveckling, miljövetenskap och teknik
Bhattacharya, Prosun, 1962- (författare)
KTH,Hållbar utveckling, miljövetenskap och teknik
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 (creator_code:org_t)
Elsevier, 2020
2020
Engelska.
Ingår i: Science of the Total Environment. - : Elsevier. - 0048-9697 .- 1879-1026. ; 715
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • Elevated Arsenic (As) and Fluoride (F) concentrations in groundwater have been studied in the shallow aquifers of northeastern of La Pampa province, in the Chaco-Pampean plain, Argentina. The source of As and co-contaminants is mainly geogenic, from the weathering of volcanic ash and loess (rhyolitic glass) that erupted from the Andean volcanic range. In this study we have assessed the groundwater quality in two semi-arid areas of La Pampa. We have also identified the spatial distribution of As and co-contaminants in groundwater and determined the major factors controlling the mobilization of As in the shallow aquifers. The groundwater samples were circum-neutral to alkaline (7.4 to 92), oxidizing (Eh similar to 0.24 V) and characterized by high salinity (EC = 456-11,400 mu S/cm) and Na+-HCO3- water types in recharge areas. Carbonate concretions ("tosca") were abundant in the upper layers of the shallow aquifer. The concentration of total As (5.6 to 535 mu g/L) and F (0.5 to 14.2 mg/L) were heterogeneous and exceeded the recommended WHO Guidelines and the Argentine Standards for drinking water. The predominant As species were arsenate As(V) oxyanions, determined by thermodynamic calculations. Arsenic was positively correlated with bicarbonate (HCO3-), fluoride (F), boron (B) and vanadium (V), but negatively correlated with iron (Fe), aluminium (Al), and manganese (Mn), which were present in low concentrations. The highest amount of As in sediments was from the surface of the dry lake. The mechanisms for As mobilization are associated with multiple factors: geochemical reactions, hydrogeological characteristics of the local aquifer and climatic factors. Desorption of As(V) at high pH, and ion competition for adsorption sites are considered the principal mechanisms for As mobilization in the shallow aquifers. In addition, the long-term consumption of the groundwater could pose a threat for the health of the local community and low cost remediation techniques are required to improve the drinking water quality.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences (hsv//eng)

Nyckelord

Arsenic
Fluoride
Shallow groundwater
La Pampa
Loess sediments
Volcanic ash

Publikations- och innehållstyp

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art (ämneskategori)

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